Jump to content

Zinnwaldite

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by The Nth User (talk | contribs) at 21:36, 19 May 2019 (References: Replaced one category with subcategory). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Zinnwaldite
Fluorapatite with topaz on zinnwaldite and quartz
General
CategoryPhyllosilicate mineral
Formula
(repeating unit)
KLiFeAl(AlSi3)O10(OH,F)2
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
(same H-M symbol)
Unit cella = 5.29, b = 9.14
c = 10.09 [Å]; β = 100.83°
Identification
ColorGray-brown, yellow-brown, pale violet, dark green, color zoning common
Crystal habitWell-formed short prismatic or tabular crystals, pseudohexagonal, in rosettes or fan-shaped groups; lamellar or scaly aggregates; disseminated.
TwinningOn composition plane {001}, twin axis [310]
CleavagePerfect basal {001}
FractureUneven
TenacityLaminae °exible, elastic
Mohs scale hardness3.5 - 4.0
LusterPearly to vitreous
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity2.9 - 3.1
Optical propertiesBiaxial (-)
Refractive indexnα = 1.565 - 1.625 nβ = 1.605 - 1.675 nγ = 1.605 - 1.675
Birefringence0.040 - 0.050
PleochroismDistinct, X = colorless to yellow-brown; Y = gray-brown; Z = colorless to gray-brown
2V angle0 - 40°
References[1][2][3]

Zinnwaldite, KLiFeAl(AlSi3)O10(OH,F)2, potassium lithium iron aluminium silicate hydroxide fluoride is a silicate mineral in the mica group. The IMA status is as a series between siderophyllite (KFe2Al(Al2Si2)O10(F,OH)2) and polylithionite (KLi2AlSi4O10(F,OH)2) and not considered a valid mineral species.[3]

Name and discovery

It was first described in 1845 in Zinnwald/Cinovec on the German-Czech Republic border.[3]

Occurrence

It occurs in greisens, pegmatite, and quartz veins often associated with tin ore deposits. It is commonly associated with topaz, cassiterite, wolframite, lepidolite, spodumene, beryl, tourmaline, and fluorite.[1]

References